Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph

The main outlets of karst systems are springs, the hydrographs of which are largely affected by flow processes in the unsaturated zone. These processes differ between the epikarst and transmission zone on the one hand and the matrix and conduit on the other hand. However, numerical models rarely con...

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Main Authors: Lucie Dal Soglio, Charles Danquigny, Naomi Mazzilli, Christophe Emblanch, Gérard Massonnat
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/11/3221
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spelling doaj-5c4e3229b07042e285900f702960806b2020-11-25T04:07:29ZengMDPI AGWater2073-44412020-11-01123221322110.3390/w12113221Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet HydrographLucie Dal Soglio0Charles Danquigny1Naomi Mazzilli2Christophe Emblanch3Gérard Massonnat4Avignon Université, INRAE, UMR EMMAH, F-84000 Avignon, FranceAvignon Université, INRAE, UMR EMMAH, F-84000 Avignon, FranceAvignon Université, INRAE, UMR EMMAH, F-84000 Avignon, FranceAvignon Université, INRAE, UMR EMMAH, F-84000 Avignon, FranceTotal, CSTJF, Avenue Larribau, 64018 Pau CEDEX, FranceThe main outlets of karst systems are springs, the hydrographs of which are largely affected by flow processes in the unsaturated zone. These processes differ between the epikarst and transmission zone on the one hand and the matrix and conduit on the other hand. However, numerical models rarely consider the unsaturated zone, let alone distinguishing its subsystems. Likewise, few models represent conduits through a second medium, and even fewer do this explicitly with discrete features. This paper focuses on the interest of hybrid models that take into account both unsaturated subsystems and discrete conduits to simulate the reservoir-scale response, especially the outlet hydrograph. In a synthetic karst aquifer model, we performed simulations for several parameter sets and showed the ability of hybrid models to simulate the overall response of complex karst aquifers. Varying parameters affect the pathway distribution and transit times, which results in a large variety of hydrograph shapes. We propose a classification of hydrographs and selected characteristics, which proves useful for analysing the results. The relationships between model parameters and hydrograph characteristics are not all linear; some of them have local extrema or threshold limits. The numerous simulations help to assess the sensitivity of hydrograph characteristics to the different parameters and, conversely, to identify the key parameters which can be manipulated to enhance the modelling of field cases.https://www.mdpi.com/2073-4441/12/11/3221karsthydrodynamicsunsaturated zonevadose zonehybrid modelnumerical experiments
collection DOAJ
language English
format Article
sources DOAJ
author Lucie Dal Soglio
Charles Danquigny
Naomi Mazzilli
Christophe Emblanch
Gérard Massonnat
spellingShingle Lucie Dal Soglio
Charles Danquigny
Naomi Mazzilli
Christophe Emblanch
Gérard Massonnat
Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph
Water
karst
hydrodynamics
unsaturated zone
vadose zone
hybrid model
numerical experiments
author_facet Lucie Dal Soglio
Charles Danquigny
Naomi Mazzilli
Christophe Emblanch
Gérard Massonnat
author_sort Lucie Dal Soglio
title Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph
title_short Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph
title_full Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph
title_fullStr Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph
title_full_unstemmed Taking into Account both Explicit Conduits and the Unsaturated Zone in Karst Reservoir Hybrid Models: Impact on the Outlet Hydrograph
title_sort taking into account both explicit conduits and the unsaturated zone in karst reservoir hybrid models: impact on the outlet hydrograph
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-11-01
description The main outlets of karst systems are springs, the hydrographs of which are largely affected by flow processes in the unsaturated zone. These processes differ between the epikarst and transmission zone on the one hand and the matrix and conduit on the other hand. However, numerical models rarely consider the unsaturated zone, let alone distinguishing its subsystems. Likewise, few models represent conduits through a second medium, and even fewer do this explicitly with discrete features. This paper focuses on the interest of hybrid models that take into account both unsaturated subsystems and discrete conduits to simulate the reservoir-scale response, especially the outlet hydrograph. In a synthetic karst aquifer model, we performed simulations for several parameter sets and showed the ability of hybrid models to simulate the overall response of complex karst aquifers. Varying parameters affect the pathway distribution and transit times, which results in a large variety of hydrograph shapes. We propose a classification of hydrographs and selected characteristics, which proves useful for analysing the results. The relationships between model parameters and hydrograph characteristics are not all linear; some of them have local extrema or threshold limits. The numerous simulations help to assess the sensitivity of hydrograph characteristics to the different parameters and, conversely, to identify the key parameters which can be manipulated to enhance the modelling of field cases.
topic karst
hydrodynamics
unsaturated zone
vadose zone
hybrid model
numerical experiments
url https://www.mdpi.com/2073-4441/12/11/3221
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